Wet‐Snow Metamorphism Drives the Transition From Preferential to Matrix Flow in Snow-Reference-Cited by-同舟云学术

Wet‐Snow Metamorphism Drives the Transition From Preferential to Matrix Flow in Snow

Published:2019-12-27 Issue:24 Volume:46 Page:14548-14557
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Hirashima Hiroyuki¹,Avanzi Francesco²³,Wever Nander⁴

Affiliation:

1. Snow and Ice Research Center National Research Institute for Earth Science and Disaster Resilience Nagaoka Japan

2. Department of Civil and Environmental Engineering University of California Berkeley CA USA

3. CIMA Research Foundation Savona Italy

4. Department of Atmospheric and Oceanic Sciences University of Colorado Boulder Boulder CO USA

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL084152

Reference51 articles.

1. Adachi S. S.Yamaguchi T.Ozeki andK.Kose(2012).Hysteresis in the water retention curve of snow measured using an MRI system inProceedings of the 2012 International Snow Science Workshop. Grenoble France.

2. Observations of capillary barriers and preferential flow in layered snow during cold laboratory experiments

3. Early formation of preferential flow in a homogeneous snowpack observed by micro-CT

4. Characteristics of wet-snow avalanche activity: 20 years of observations from a high alpine valley (Dischma, Switzerland)

5. Laboratory Tests of a Theory of Fingering during Infiltration into Layered Soils

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